The Moon: considered as a planet, a world, and a satellite.Nasmyth, James
Science
The Moon: considered as a planet, a world, and a satellite.
Nasmyth, James
Moon
Although we cannot, obviously, see upon the moon evidence of a cone
actually overtopped by the rising lake of lava, yet it is not
unreasonable to suppose that such a condition of things actually
occurred in many of those instances in which we observe craters without
central cones, but with plateaux so smooth as to indicate previous
fluidity or viscosity. From the state of things exhibited in Fig. 25 the
transition to that shewn in Fig. 27 is easily, and to our view
reasonably, conceivable. We are in a manner led up to this idea by a
review of the various heights of central cones above their surrounding
plateaux. For instance, in such examples as Tycho or Theophilus, we have
cones high above the lava floor; in Copernicus, Arzachael and Alphonsus
they are comparatively lower; the lava in these and some other craters
does not appear to have risen so high; while in Aristotle and Eudoxus
among others, we have only traces of cones, and it is supposable that in
these cases the lava rose so high as nearly to overtop the central
cones. Why should it not have risen so far as to overtop and therefore
conceal some cones entirely? We offer this as at least a feasible
explanation of some coneless craters: it is not necessary to suppose
that it applies to all such, however: there may have been many craters,
the formation of which ceased so abruptly that no cone was produced,
though the welling forth of lava occurred from the vent, which may have
been left fully open, as in Fig. 28, or so far choked as to stay the
egress of solid ejecta and yet allow the fluid material to ooze upwards
through it, and so form a lake of molten lava which on consolidation
became the plateau. As most of the examples of coneless craters exhibit
on careful examination minute craters on the surface of the otherwise
smooth plateaux, we may suppose that such minute craters are evidences
of the upflow of lava which resulted in the plateaux.
[Illustration: PLATE X.
ARISTOTLE & EUDOXUS.]
[Illustration: Fig. 26.]
[Illustration: Fig. 27.]
[Illustration: Fig. 28.]
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